TY - JOUR
T1 - Investigation of a mesospheric gravity wave ducting event using coordinated sodium lidar and Mesospheric Temperature Mapper measurements at ALOMAR, Norway (69°N)
AU - Bossert, Katrina
AU - Fritts, David C.
AU - Pautet, Pierre Dominique
AU - Taylor, Michael J.
AU - Williams, Bifford P.
AU - Pendelton, William R.
N1 - Funding Information:
The Weber sodium lidar research at ALOMAR was supported by the National Science Foundation under grants AGS-1136269 and AGS-1259136. The lidar was originally developed and installed at ALOMAR with AFOSR DURIP funding to C.-Y. She at CSU. The design and initial development of the AMTM was supported under a separate AFOSR DURIP grant to M. Taylor at the USU Research Foundation, and we gratefully acknowledge R. Esplin and D. Mclain for their expertise and help in its development and testing. The AMTM installation and current operations at ALOMAR are supported under an NSF collaborative grant AGS-1042227. We also acknowledge facility support by the Institute of Atmospheric Physics in Germany.
Funding Information:
The Weber sodium lidar research at ALOMAR was supported by the National Science Foundation under grants AGS‐1136269 and AGS‐1259136. The lidar was originally developed and installed at ALOMAR with AFOSR DURIP funding to C.‐Y. She at CSU. The design and initial development of the AMTM was supported under a separate AFOSR DURIP grant to M. Taylor at the USU Research Foundation, and we gratefully acknowledge R. Esplin and D. Mclain for their expertise and help in its development and testing. The AMTM installation and current operations at ALOMAR are supported under an NSF collaborative grant AGS‐1042227. We also acknowledge facility support by the Institute of Atmospheric Physics in Germany.
Publisher Copyright:
©2014. American Geophysical Union. All Rights Reserved.
PY - 2014/8/27
Y1 - 2014/8/27
N2 - New measurements at the ALOMAR observatory in northern Norway (69°N, 16°E) using the Weber sodium lidar and the Advanced Mesospheric Temperature Mapper (AMTM) allow for a comprehensive investigation of a gravity wave (GW) event on 22 and 23 January 2012 and the complex and varying propagation environment in which the GW was observed. These observational techniques provide insight into the altitude ranges over which a GW may be evanescent or propagating and enable a clear distinction in specific cases. Weber sodium lidar measurements provide estimates of background temperature, wind, and stability profiles at altitudes from ~78 to 105 km. Detailed AMTM temperature maps of GWs in the OH emission layer together with lidar measurements quantify estimates of the observed and intrinsic GW parameters centered near 87 km. Lidar measurements of sodium densities also allow more precise identification of GW phase structures extending over a broad altitude range. We find for this particular event that the extent of evanescent regions versus regions allowing GW propagation can vary largely over a period of hours and significantly change the range of altitudes over which a GW can propagate.
AB - New measurements at the ALOMAR observatory in northern Norway (69°N, 16°E) using the Weber sodium lidar and the Advanced Mesospheric Temperature Mapper (AMTM) allow for a comprehensive investigation of a gravity wave (GW) event on 22 and 23 January 2012 and the complex and varying propagation environment in which the GW was observed. These observational techniques provide insight into the altitude ranges over which a GW may be evanescent or propagating and enable a clear distinction in specific cases. Weber sodium lidar measurements provide estimates of background temperature, wind, and stability profiles at altitudes from ~78 to 105 km. Detailed AMTM temperature maps of GWs in the OH emission layer together with lidar measurements quantify estimates of the observed and intrinsic GW parameters centered near 87 km. Lidar measurements of sodium densities also allow more precise identification of GW phase structures extending over a broad altitude range. We find for this particular event that the extent of evanescent regions versus regions allowing GW propagation can vary largely over a period of hours and significantly change the range of altitudes over which a GW can propagate.
KW - gravity wave ducting
KW - mesospheric dynamics
KW - mesospheric remote sensing
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U2 - 10.1002/2014JD021460
DO - 10.1002/2014JD021460
M3 - Article
AN - SCOPUS:84944912319
VL - 119
SP - 9765
EP - 9778
JO - Journal of Geophysical Research: Atmospheres
JF - Journal of Geophysical Research: Atmospheres
SN - 2169-897X
IS - 16
ER -